Titlebook: Meteorology for Coastal Scientists; Robert V. Rohli,Chunyan Li Textbook 2021 Springer Nature Switzerland AG 2021 Air-Sea Interaction.Air-S

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Inelasticity

Energy Transfer and Electromagnetic Radiationr importance is electromagnetic radiation—the mechanism by which energy from the Sun crosses through space and enters Earth’s atmosphere. Laws governing the intensity of this solar (shortwave) radiation can tell us the wavelength of peak intensity, the energy emitted at a particular wavelength, and

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Temperaturenly used to measure temperature and terms used to describe the temperature of a place. The diurnal cycle of temperature on a “typical” day is then described in the context of local surpluses and deficits of radiant energy. Reasons that coastal and marine areas have markedly damped temperature compar

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The Hydrostatic Equation and Adiabatic Processes equation, which relates height differences in a static atmosphere to the vertical pressure change over those differences. In addition, the First Law of Thermodynamics—the postulate that energy can be neither created nor destroyed, but only changed from one form to another—applies by ensuring that a

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Measuring and Estimating Atmospheric Stabilityg the stability condition based on the temperature profile. A global network of sites where instrument packages called radiosondes are launched synchronously twice daily measure, among other variables, the vertical temperature profile. A less accurate, precise, and expensive method is to rank stabil

AWRY

Using Thermodynamic Diagrams in Meteorology a quick sense of the atmospheric properties. The Skew-T Log-P diagram is a type of thermodynamic diagram used by the U.S. National Weather Service. This diagram plots isotherms of temperature as lines slanted (hence, the “Skew-T”) upward from left to right. Isobars of constant pressure are shown as